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Near-resonace transverse oscillations in an elastic layer. Steady-state solutions
Authors:AG Kulikovskii  EI Sveshnikova
Institution:1. Research Centre for Animal Welfare, MTT Agrifood Research Finland, Agricultural Engineering Research, 03400 Vihti, Finland;2. INRA, Centre de Clermont-Ferrand/Theix, URH-ACS, 63122 Saint-Genès-Champanelle, France;3. INRA, Centre de Clermont-Ferrand/Theix, Domaine de Marcenat, 15190 Marcenat, France;1. Laboratoire de Geologie, École Normale Supérieure, CNRS UMR 8538, Paris, France;2. Institut TELECOM, TELECOM ParisTech, LTCI CNRS UMR 5141, 75013 Paris, France
Abstract:The solutions of the equations of the non-linear evolution of transverse oscillations in a layer of an incompressible elastic medium under conditions close to resonance conditions are investigated qualitatively and using analytical methods. The oscillations are created by a small periodic motion of one of the boundaries in its plane, with a period that is close to the period of the natural oscillations of the layer. It is assumed that the medium can possess slight anisotropy and that the amplitude of the oscillations which arise is small. Previously obtained differential equations are used, which describe the slow evolution of the wave pattern of non-linear transverse waves. Two possible formulations of problems for these equations are considered. In the first formulation, it is determined what the external action must be in order that the non-linear evolution of oscillations or periodic oscillations occurs according to a (previously specified) desired law. In the second formulation it is assumed that the periodic motion of one of the boundaries is given. It is shown that a steady-state solution, that does not vary from period to period, can be represented by a continuous solution and also by a solution which contains discontinuities in the strain and velocity components. The mechanism of the overturn of a non-linear wave during its evolution and the formation of a discontinuity are qualitatively described.
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